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现代矿业 ›› 2026, Vol. 42 ›› Issue (04): 145-150.

• 地质·测量 • 上一篇    下一篇

高精度磁法测量在南歧铁矿勘查中的应用

安瑞鹏1 王欣欣1 杨鹤鹤1 白金吉1 赵 璐1 赵 晋2   

  1. 1 .山西大同大学煤炭工程学院;2.山西省地质勘查局二一七地质队有限责任公司
  • 出版日期:2026-04-25 发布日期:2026-05-26

Application of High-precision Magnetic Survey in Nanqi Iron Ore Exploration

  1. 1 .College of Coal Engineering,Shanxi Datong University;2.217 Geological Team Co.,Ltd.,Shanxi Pro⁃ vincial Geological Prospecting Bureau
  • Online:2026-04-25 Published:2026-05-26

摘要: 为解决灵丘县南歧铁矿工作区前期物化探覆盖不足、异常数据有限等问题,需探明 磁铁矿空间分布、延伸特征及深部变化规律,为后续地质勘查提供科学指引。研究采用地面高精 度磁法测量技术,布设密集测网,采集磁异常数据,同时结合向上延拓处理,消除浅部干扰,凸显深 部矿体信息,并运用人机交互反演手段,对磁异常进行定量解析。经数据精细处理与系统分析,成 功圈定5 处显著磁异常区域,其中5#异常区呈北西向展布,长约650 m,宽100 ~370 m,异常中心ΔT≥ 20 000 nT,矿体主要赋存于向斜构造核部的翘起端及其两翼,稳定集中,延深较大,具有一定规模。 C4 异常是由矿体较集中、平行排列、埋深和延深较大、向南西倾斜的磁铁矿体所引起,虽属低缓异 常,实为北异常带随含铁岩系地层的褶曲、构造影响的东延表现。1#~3#异常区规模相对较小,延伸 不大。综合研究表明,高精度磁测技术能有效识别深部磁铁矿体的空间分布规律,圈定的异常区 为铁矿勘查靶区优选提供了可靠依据,建议优先对5#异常区开展钻探验证,为矿区资源量估算及 开发规划奠定基础。

关键词: 高精度磁法, 磁异常, 铁矿勘查

Abstract: To address the issues of insufficient coverage and limited abnormal data in the early explo ⁃ ration of the Nanqi iron mining area in Lingqiu County,it is necessary to clarify the spatial distribution, extension characteristics,and deepening patterns of the magnetite deposits,in order to provide scientific guidance for subsequent geological exploration.The study employed ground high-precision magnetic mea ⁃ surement technology,setting up a dense measurement network to collect magnetic anomaly data.At the same time,upward extension processing was used to eliminate shallow interference and highlight deep min ⁃ eral body information.The inversion method of human-computer interaction was applied to conduct quantita ⁃ tive analysis of the magnetic anomalies.Through detailed data processing and systematic analysis,5 signifi⁃ cant magnetic anomaly areas were successfully delineated.Among them,the 5#anomaly area is distributed in a north-westward direction,with a length of approximately 650 m and a width of 100 ~370 m.The anoma⁃ ly center has a ΔT ≥20 000 nT.The ore body is mainly distributed in the uplifted end of the anticline struc ⁃ ture and its two wings.The ore body is stable and concentrated,with a large extension,and has a certain scale.The C4 anomaly is caused by the relatively concentrated,parallelly arranged,deep and extended magnetite ore bodies that are inclined towards the south-west.Although it is a low-amplitude anomaly,it is actually the eastward extension of the northern anomaly belt due to the folding and structural influence of the iron-bearing rock strata.The 1#~3#anomaly areas have relatively smaller scales and shorter extensions. Comprehensive studies have shown that the high-precision magnetic survey technology can effectively iden ⁃tify the spatial distribution patterns of deep magnetite ore bodies,and the delineated anomaly areas pro ⁃ vide a reliable basis for the selection of iron ore exploration targets.It is recommended to prioritize the drill⁃ ing verification of the 5#anomaly area,laying the foundation for the estimation of the resource quantity and development planning of the mining area.

Key words: high-precision magnetic method, magnetic anomaly, iron ore exploration